Badlands Photos

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The Tree of Eons, a spectacular dendritic formation in the Bentonite Hills of Utah. Fantastic colorful sedimentary patterns, ancient Bentonite layers are exposed through erosion in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Photographed just before sunrise with soft pre-dawn illumination. Aerial panoramic photograph
The Tree of Eons, a spectacular dendritic formation in the Bentonite Hills of Utah. Fantastic colorful sedimentary patterns, ancient Bentonite layers are exposed through erosion in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Photographed just before sunrise with soft pre-dawn illumination. Aerial panoramic photograph.
Location: Utah
Image ID: 37951  
Panorama dimensions: 11000 x 15000
Dawn over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. The Henry Mountains are in the distance
Dawn over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. The Henry Mountains are in the distance.
Location: Utah
Image ID: 38025  
Pre-Dawn over the Tree of Eons, Utah. The Tree of Eons is a spectacular geologic sight near the San Rafael Swell. Erosion has cut a "tree" through red, blue, purple and white layers of the Chinle formation. The Tree of Eons is a superb example of dendritic erosion and to really appreciate the complex fractal-like details it must be observed from above. Photographed here in the soft, predawn light, it takes on magenta, red and purple hues just before the sun reaches it. Aerial panoramic photograph
Pre-Dawn over the Tree of Eons, Utah. The Tree of Eons is a spectacular geologic sight near the San Rafael Swell. Erosion has cut a "tree" through red, blue, purple and white layers of the Chinle formation. The Tree of Eons is a superb example of dendritic erosion and to really appreciate the complex fractal-like details it must be observed from above. Photographed here in the soft, predawn light, it takes on magenta, red and purple hues just before the sun reaches it. Aerial panoramic photograph.
Location: Utah
Image ID: 38027  
Fantastic colorful sedimentary patterns of Bentonite layers, seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes into layers, now revealed through erosion. Aerial photograph
Fantastic colorful sedimentary patterns of Bentonite layers, seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes into layers, now revealed through erosion. Aerial photograph.
Location: Utah
Image ID: 37947  
Erosion patterns in the Utah Badlands, aerial abstract photo, Hanksville
Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 37948  
Molly's Castle, aerial view, Goblin Valley State Park. Curtis Formation whiteish caprock is on top, with reddish Entrada Sandstone below, both of Jurassic era. Molly's castle lies in the San Rafael desert near Goblin Valley, and drains into the Colorado River watershed. Aerial panoramic photograph
Molly's Castle, aerial view, Goblin Valley State Park. Curtis Formation whiteish caprock is on top, with reddish Entrada Sandstone below, both of Jurassic era. Molly's castle lies in the San Rafael desert near Goblin Valley, and drains into the Colorado River watershed. Aerial panoramic photograph.
Location: Goblin Valley State Park, Utah
Image ID: 37950  
Self-portrait at dawn, Bentonite Hills, Utah
Self-portrait at dawn, Bentonite Hills, Utah.
Location: Utah
Image ID: 38028  
Dawn breaks over the Bentonite Hills in the Utah Badlands. Striations in soil reveal layers of the Morrison Formation, formed in swamps and lakes in the Jurassic era. Aerial panoramic photograph
Dawn breaks over the Bentonite Hills in the Utah Badlands. Striations in soil reveal layers of the Morrison Formation, formed in swamps and lakes in the Jurassic era. Aerial panoramic photograph.
Location: Utah
Image ID: 38062  
Molly's Castle, aerial view, Goblin Valley State Park, Mollys Castle
Molly's Castle, aerial view, Goblin Valley State Park.
Location: Mollys Castle, Goblin Valley State Park, Utah
Image ID: 38016  
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Aerial photograph
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Aerial photograph.
Location: Utah
Image ID: 38029  
Lower Blue Hills Badlands, sunrise, Utah
Lower Blue Hills Badlands, sunrise, Utah.
Location: Utah
Image ID: 38031  
Factory Butte at sunrise. An exceptional example of a solitary butte surrounded by dramatically eroded badlands, Factory Butte stands alone on the San Rafael Swell, Hanksville, Utah
Factory Butte at sunrise. An exceptional example of a solitary butte surrounded by dramatically eroded badlands, Factory Butte stands alone on the San Rafael Swell.
Location: Factory Butte, Hanksville, Utah
Image ID: 38054  
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands, part of the Chinle Formation formed during the Upper Triassic Period. Aerial photograph
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands, part of the Chinle Formation formed during the Upper Triassic Period. Aerial photograph.
Location: Utah
Image ID: 38177  
Factory Butte at sunrise, aerial photo, Utah. An exceptional example of solitary butte surrounded by dramatically eroded badlands, Factory Butte stands alone on the San Rafael Swell, Hanksville
Factory Butte at sunrise, aerial photo, Utah. An exceptional example of solitary butte surrounded by dramatically eroded badlands, Factory Butte stands alone on the San Rafael Swell.
Location: Factory Butte, Hanksville, Utah
Image ID: 38076  
Hoodoos in Goblin Valley State Park, aerial panorama. The "goblins" are technically known as hoodoos, formed through the gradual erosion of Entrada sandstone deposited 170 millions years ago. Aerial panoramic photograph
Hoodoos in Goblin Valley State Park, aerial panorama. The "goblins" are technically known as hoodoos, formed through the gradual erosion of Entrada sandstone deposited 170 millions years ago. Aerial panoramic photograph.
Location: Goblin Valley State Park, Utah
Image ID: 37957  
Erosion patterns in the Utah Badlands, aerial abstract photo, Hanksville
Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38017  
Erosion patterns in the Utah Badlands, aerial abstract photo, Hanksville
Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38018  
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands, part of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Aerial photograph
Fantastic colorful sedimentary patterns, Bentonite layers are seen as striations exposed in the Utah Badlands, part of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Aerial photograph.
Location: Utah
Image ID: 38019  
Sunrise over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. The San Rafael Swell is in the distance
Sunrise over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. The San Rafael Swell is in the distance.
Location: Utah
Image ID: 38026  
Erosion patterns in the Utah Badlands, aerial abstract photo, Hanksville
Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38032  
Dawn over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. Factory Butte is in the distance
Dawn over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. Factory Butte is in the distance.
Location: Utah
Image ID: 38064  
Dawn breaks over the Bentonite Hills in the Utah Badlands. Striations in soil reveal layers of the Morrison Formation, formed in swamps and lakes in the Jurassic era. Aerial panoramic photograph
Dawn breaks over the Bentonite Hills in the Utah Badlands. Striations in soil reveal layers of the Morrison Formation, formed in swamps and lakes in the Jurassic era. Aerial panoramic photograph.
Location: Utah
Image ID: 38065  
Hoodoos in Goblin Valley State Park. The "goblins" are technically known as hoodoos, formed through the gradual erosion of Entrada sandstone deposited 170 millions years ago
Hoodoos in Goblin Valley State Park. The "goblins" are technically known as hoodoos, formed through the gradual erosion of Entrada sandstone deposited 170 millions years ago.
Location: Goblin Valley State Park, Utah
Image ID: 38066  
Fantastic colorful sedimentary patterns of Bentonite layers, seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes into layers, now revealed through erosion. Aerial photograph
Fantastic colorful sedimentary patterns of Bentonite layers, seen as striations exposed in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes into layers, now revealed through erosion. Aerial photograph.
Location: Utah
Image ID: 38067  
Lower Blue Hills Badlands, sunrise, Utah
Lower Blue Hills Badlands, sunrise, Utah.
Location: Utah
Image ID: 38074  
Erosion patterns in the Utah Badlands, aerial abstract photo, Hanksville
Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38170  
Erosion patterns in the Utah Badlands, aerial abstract photo, Hanksville
Erosion patterns in the Utah Badlands, aerial abstract photo.
Location: Hanksville, Utah
Image ID: 38173  
Mars Desert Research Station, set amid beautiful Mars-like "Bentonite Hills", near Hanksville, Utah
Mars Desert Research Station, set amid beautiful Mars-like "Bentonite Hills", near Hanksville, Utah.
Location: Utah
Image ID: 38179  
Lower Blue Hills Badlands, sunrise, Utah
Lower Blue Hills Badlands, sunrise, Utah.
Location: Utah
Image ID: 38180  
White Cap Mesa overlooking Goblin Valley State Park, Utah
White Cap Mesa overlooking Goblin Valley State Park, Utah.
Location: Goblin Valley State Park, Utah
Image ID: 38182  
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All photographs copyright © Phillip Colla / Oceanlight.com, all rights reserved worldwide.